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在CFG桩复合地基中, 褥垫层的设置厚度和模量对于复合地基的承载及变形特性有较大的影响。本文建立了CFG桩复合地基的三维弹塑性数值分析模型,研究了当采用不同厚度和模量的褥垫层时,复合地基沉降、桩端沉降、褥垫层压缩量和桩土应力等参数的变化规律。结果表明复合地基沉降和褥垫层压缩量随着垫层厚度的增加而增大,而随着垫层模量的增大而减小;垫层厚度和模量的变化对于桩端沉降的影响较小,从工程角度可认为桩端沉降不随垫层厚度与垫层模量的变化而变化;桩土应力比随垫层厚度的增大而减小,随垫层模量的增大而增大。本文建立的分析模型还可进一步对CFG桩复合地基的其他参数进行相应的分析计算,分析结果可以为复合地基的设计和施工提供相应的理论依据。 相似文献
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分析了刚性桩复合地基中垫层、桩及桩间土的共同作用机理,考虑复合地基中桩、土变形协调,提供一种计算复合地基桩土应力比的方法;在此基础上研究复合地基中垫层模量、桩端持力层模量、桩土相对刚度比、桩长径比、面积置换率等因素对复合地基桩土应力比的影响,分析刚性桩复合地基的承载特性。 相似文献
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CFG桩复合地基受力性状三维数值模拟研究 总被引：3，自引：0，他引：3
以工程应用实例为背景,运用有限差分法数值模拟方法分析了在分级加载工况下CFG桩单桩及复合地基的变形和受力特征,模拟了桩-土共同承担荷载的复合效应以及褥垫层的效用.模拟结果表明,将具有刚性桩特点的CFG桩以一定的密度置入地基土中,可以有效地提高原地基土的承载能力,桩体应力发挥丰要集中在1/2桩长范围之内,适当加大桩长有助于控制地基变形,同时桩顶褥垫层的设置对于调整桩-土应力的分担起到了积极的作用,该分析方法及模拟成果对于类似工程具有一定的参考价值. 相似文献
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刚性基础下现浇X形桩复合地基桩-土应力比分析 总被引：3，自引：2，他引：1
桩土应力比是反映复合地基承载特性的重要参数之一,可反映复合地基的荷载传递和变形机制。做为一种新型桩,目前尚未得出统一的计算X形桩复合地基桩土应力比的公式。沉淀池、滤池等构筑物是典型的具有混凝土底板（刚性基础）的结构,刚性基础下桩复合地基的承载性能有别于柔性基础。故结合南京桥北污水处理厂地基处理工程做现场静载荷试验,应用有限元软件ABAQUS建立刚性荷载板下现浇X形混凝土桩复合地基的模型,模拟不同桩身弹性模量、桩周土压缩模量、桩长、褥垫层厚度和压缩模量等参数下现浇X形混凝土桩复合地基的桩土应力比,结果表明,桩身或褥垫层模量增大、桩周土体模量减小、褥垫层厚度减小、桩长等增加都能使桩土应力比增大;现浇X形桩复合地基桩土应力比理想值为20～25,此时桩身模量取10～20 GPa,碎石褥垫层的厚度为20～40 cm,模量为30～45 MPa。 相似文献
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考虑桩端刺入沉降的桩土自平衡式复合地基设计 总被引：2，自引：0，他引：2
复合地基的本质是增强体与地基土通过变形协调共同承担上覆荷载。褥垫层的设置起到了协调桩土变形的作用,但褥垫层工作性状及变形特性尚不明确,其厚度设计仍然参考规范依靠经验判断,往往不能充分发挥地基土的承载作用。目前复合地基设计通常采用褥垫层调节桩土变形,而忽略了桩端刺入沉降协调桩土变形来发挥地基土的承载作用,为了利用桩端刺入沉降协调桩土变形,充分发挥桩间土承载的作用,减薄褥垫层或不设褥垫层并减小设计桩长,以期降低地基处理费用,实现桩土共同承担荷载的目的,建立了通过控制桩端刺入沉降协调桩土变形的自平衡式复合地基设计方法。通过与褥垫层方法对比以及工程实例计算,结果表明,该方法可更好地发挥桩土承载作用,为复合地基优化设计提供参考。 相似文献
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CFG桩复合地基褥垫层效用的有限元分析 总被引：12，自引：2，他引：10
复合地基上褥垫层的设计是桩体复合地基设计的关键技术,通过有限元数值模拟分析,得到了桩土沉降与荷载之间的关系,获得了褥垫层厚度及其压缩模量对桩土应力比、桩土沉降等的影响规律。该研究为复合地基褥垫层厚度的设置及选择和配制合理的垫层材料提供了依据,有利于复合地基的优化设计。 相似文献
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Emily Keeble David I. Whiteside Michael J. Benton 《Proceedings of the Geologists' Association. Geologists' Association》2018,129(2):99-119
Pant-y-ffynnon Quarry in South Wales yielded a rich cache of fossils in the early 1950s, including articulated specimens of new species (the small sauropodomorph dinosaur Pantydraco caducus and the crocodylomorph Terrestrisuchus gracilis), but no substantial study of the wider fauna of the Pant-y-ffynnon fissure systems has been published. Here, our overview of existing specimens, a few described but mostly undescribed, as well as freshly processed material, provides a comprehensive picture of the Pant-y-ffynnon palaeo-island of the Late Triassic. This was an island with a relatively impoverished fauna dominated by small clevosaurs (rhynchocephalians), including a new species, Clevosaurus cambrica, described here from a partially articulated specimen and isolated bones. The new species has a dental morphology that is intermediate between the Late Triassic Clevosaurus hudsoni, from Cromhall Quarry to the east, and the younger C. convallis from Pant Quarry to the west, suggesting adaptive radiation of clevosaurs in the palaeo-archipelago. The larger reptiles on the palaeo-island do not exceed 1.5?m in length, including a small carnivorous crocodylomorph, Terrestrisuchus, and a possible example of insular dwarfism in the basal dinosaur Pantydraco. 相似文献
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Gilles Serge Odin 《Comptes Rendus Geoscience》2002,334(6):409-414
Lithostratigraphy, physicochemical stratigraphy, biostratigraphy, and geochronology of the 77–70 Ma old series bracketing the Campanian–Maastrichtian boundary have been investigated by 70 experts. For the first time, direct relationships between macro- and microfossils have been established, as well as direct and indirect relationships between chemo-physical and biostratigraphical tools. A combination of criteria for selecting the boundary level, duration estimates, uncertainties on durations and on the location of biohorizons have been considered; new chronostratigraphic units are proposed. The geological site at Tercis is accepted by the Commission on Stratigraphy as the international reference for the stratigraphy of the studied interval. To cite this article: G.S. Odin, C. R. Geoscience 334 (2002) 409–414. 相似文献
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The effect of water on accessory phase solubility in subaluminous and peralkaline granitic melts 总被引：4，自引：0，他引：4
The solubilities of columbite, tantalite, wolframite, rutile, zircon and hafnon were determined as a function of the water contents in peralkaline and subaluminous granite melts. All experiments were conducted at 1035 °C and 2 kbar and the water contents of the melts ranged from nominally dry to approximately 6 wt.% H2O. Accessory phase solubilities are not affected by the water content of the peralkaline melt. By contrast, solubilities are affected by the water content of the subaluminous melt, where the solubilities of all the accessory phases examined increase with the water content of the melt, up to 2 wt.% H2O. At higher water contents, solubilities are nearly constant. It can be concluded that water is not an important control of accessory phase solubility, although the water content will affect diffusivities of components in the melt, thus whether or not accessory phases will be present as restite material. The solubility behaviour in the subaluminous and peralkaline melts supports previous spectroscopic studies, which have observed differences in the coordination of high field strength elements in dry vs. wet subaluminous granitic glasses, but not for peralkaline granitic glasses. Lastly, the fact that wolframite solubility increases with increasing water content in the subaluminous melt suggests that tungsten dissolved as a hexavalent species. 相似文献
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Muriel Rocher Stéphane Baize Stéphane Jaillet Edward Marc Cushing Yannick Lozac&#x;h Francis Lemeille 《Comptes Rendus Geoscience》2003,335(8):701-708
Calcite samples were extracted both from the rock matrix and the superficial coating of a karstified fault plane of an underground quarry, located in the eastern border of the Paris basin. The karstification is dated as Quaternary. Analysis of mechanical calcite twinning reveals that only the calcite matrix has also undergone a compression trending WNW that can be attributed to the Mio-Pliocene alpine collision. Both coating and matrix have undergone a strike-slip regime with σ1 roughly trending north–south, that could correspond to the regional present-day state of stress, a strike-slip compression rather trending NNW, modified by local phenomena. To cite this article: M. Rocher et al., C. R. Geoscience 335 (2003). 相似文献
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正20141520 Bo Ying(Key Laboratory of Metallogeny and Mineral Assessment,MLR,Beijing 100037,China);Liu Chenglin Saline Spring Hydrochemical Characteristics and Indicators for Potassium Exploration in Southwestern and Northern Tarim Basin,Xinjiang(Acta Geoscientica Sinica,ISSN1006-3021,CN11-3474/P,34(5),2013,p.594-602,5 illus.,3 tables,28 refs.) 相似文献
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正20141243Chen Ge(Hangzhou Research Institute of Petroleum Geology,PetroChina,Hangzhou 310023,China);Si Chunsong Study on Sedimentary Numerical Simulation Method of Fan Delta Sand Body(Journal of Geology, 相似文献
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正20142599Chen Sanming(Guangxi Key Laboratory of Concealed Deposits Exploration,Guilin University of Technology,Guilin541004,China);He Yuzhou Block Model and Reserves Estimation of Panzhihua Iron Deposit Based on 3D Geological Modeling(Journal of Guilin University of Technology,ISSN1674-9057,CN45-1375/N,33(4),2013,p.610-615,9illus.,1table,15refs.) 相似文献
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正20140594 Bai Daoyuan(Hunan Institute of Geology Survey,Changsha 410016,China);Zhong Xiang Faults in the Jingzhou Basin and Their Tectonic Settings(Geotectonica et Metallogenia,ISSN1001-1552,CN44-1595/P,37(2),2013,p.173-183,6illus.,59refs.)Key words:basin evolution,tectonic setting,South China In the Upper Paleozoic and Jurassic se- 相似文献
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正20141912Cao Hui(State Key Laboratory for Continental Tectonics and Dynamics,Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China)Gravitational Collapse and Folding during Orogenesis:A Comparative Study of FIA Trends and Fold Axial Plane Traces(Geology in China,ISSN1000-3657,CN11-1167/P,40(6),2013,p.1818-1828,9illus.,35refs.,with 相似文献